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湖南古丈县双溪钒矿床地质特征及成矿机制初探
引用本文:刘光昭,尹华锋,付益平.湖南古丈县双溪钒矿床地质特征及成矿机制初探[J].地质与资源,2007,16(3):196-199,208.
作者姓名:刘光昭  尹华锋  付益平
作者单位:湖南省有色地质勘查局二四五队, 湖南 吉首 416007
摘    要:湖南双溪钒矿床产于寒武系下统木昌组,赋矿岩层为一套富含有机质的硅、磷、碳组合的黑色岩系.钒矿(V2O5)的品位为0.61%~1.51%,矿石主要分为3种类型:黑色碳硅质岩-页岩型、含磷结核页岩型及页岩型.钒的赋存状态主要有吸附态和类质同象态.通过对成岩、成矿的研究,初步认为双溪钒矿为海底喷气热水溶液同生沉积生成.

关 键 词:钒矿床  成矿机制  双溪  湖南古丈  
文章编号:1671-1947(2007)03-0196-05
收稿时间:2006-11-24

A PRELIMINARY STUDY ON GEOLOGY AND METALLOGENESIS OF THE SHUANGXI VANADIUM DEPOSIT IN HUNAN PROVINCE
LIU Guang-zhao,YIN Hua-feng,FU Yi-ping.A PRELIMINARY STUDY ON GEOLOGY AND METALLOGENESIS OF THE SHUANGXI VANADIUM DEPOSIT IN HUNAN PROVINCE[J].Geology and Resources,2007,16(3):196-199,208.
Authors:LIU Guang-zhao  YIN Hua-feng  FU Yi-ping
Institution:NO. 245 Brigade, Hunan Bureau of Nonferrous Metallic Geologic Exploration, Jishou 416007, Hunan Province, China
Abstract:The Shuangxi vanadium deposit in Guzhang County,Hunan Province occurs in Lower Cambrian Muchang formation,which is composed of the black rock series rich in organic Si,P and C.The content of V2O5 in the ore ranges from 0.61% to 1.51%.The ore rocks can be divided into three types,i.e.black carbonaceous-siliceous rock-shale,phosphatic nodule-bearing shale and shale.The occurrences of vanadium are mainly in adsorption and isomorphism states.Study on diagenesis and metallogenesis shows that the Shuangxi vanadium deposit is formed by the syndepositon of submarine exhalative hydrothermal solution.
Keywords:vanadium deposit  metallogenic mechanism  Shuangxi of Guzhang County  Hunan Province  
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